Aquifer

Aquifer The aquifer that can be found in the cross piece A-B is a confined aquifer. It has and upper stuffy shape of moody black shale, with a weightiness of 61 meters. The lower near floor is composed of dense gray shale and has a weightiness of 3 meters. The aquifers itself is a layered heterogeneity measuring 40 meters in thickness. It is composed of three different layers; a coarse, well-cemented sandstone, 13 meters thick, a poorly-cemented coarse siltstone, 13 meters thick and a layer of poorly-cemented, fine sandstone which is 14 meters thick. The ground water flows to the southeast, or N 108 E(Base map). The aquifer has a hydraulic conductivity of 3.02 x 10-11 cm/s (Appendix A).

The hydraulic gradient (dh/dl) is 8.04 x 10-2 (Appendix A). The discharge through a 10 meter width of this aquifer would be 9.7 x 10-2 cm3/s (Appendix A). Bibliography: ...If you want to get a full essay, order it on our website: OrderEssay.net

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